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Structural behavior of Al³⁺ in peralkaline, metaluminous, and peraluminous silicate melts and glasses at ambient pressure

¹ Geophysical Laboratory, Carnegie Institution of Washington, 5251 Broad Branch Road, NW, Washington D.C. 20015, U.S.A.
² Laboratoire Dynamique Terrestre et Planétaire (UMR5562), Observatoire Midi-Pyrénées, 14 Avenue Belin, Toulouse, 31400, France

Correspondence: ^* E-mail: bmysen{at}ciw.edu

Peralkaline and peraluminous glasses close to the metaluminous join in the systems Na₂O-Al₂O₃-SiO₂ (NAS), CaO-Al₂O₃-SiO₂ (CAS), and MgO-Al₂O₃-SiO₂ (MAS) have been examined with Raman spectroscopy. At least three different SiO₂ contents in each of the systems (NAS, CAS, and MAS) have been studied. Each series of glasses spans the metaluminous join at constant silica content. The spectra of glasses in all three systems show changes consistent with a continuous decrease in abundance of depolymerized species and an increase in fully polymerized species as compositions change from peralkaline to peraluminous. There is no evidence for maxima or minima of these abundances across the metaluminous joins for any of the studied series. These observations confirm previous suggestions that non-bridging O atoms are a general feature of "fully polymerized" glasses, and that a population of Al exists in the melt structure that is not associated with a charge-balancing cation, even in peralkaline compositions.

With decreasing peralkalinity, new components appear in the Raman spectra of peraluminous NAS and CAS glasses, but such changes are much less obvious in the MAS system. These additional components are most likely related to the presence of "excess" Al (i.e., Al not associated with a charge-balancing cation). The structural role of this "excess" Al could be in the form of (Al, Si)-triclusters with different Al/Si-ratios depending on composition, but simple distorted AlO₄-tetrahedra and possibly higher-coordinate Al³⁺ cannot be ruled out from the Raman spectra alone. The implications of these results for isothermal variations in viscosity are considered. It is concluded that the diversity and complexity of viscosity variations observed in different aluminosilicate systems may be a consequence of the fact that the difference in bond strength between bridging and non-bridging O atoms in the Ca and Mg-bearing systems is small compared to that in the Na-bearing system.

Key Words: Melt structure • aluminosilicate • spectroscopy • Raman